Corrennie Granite

Corrennie Granite was sourced from at least three quarries near the village of Tillyfourie, in Aberdeenshire. The stone comes from the Corrennie Granite Intrusion, which formed during the Ordovician Period (c. 450 million years ago) when Scotland was south of the Equator at roughly the same latitude as northern Angola is today. Corrennie Granite was used locally, regionally and nationally, mainly to form masonry. Corrennie Granite is not quarried for building stone today.

Geological description

Source bedrock unit  
Corrennie Granite Intrusion
Colour  
Bright orange and medium grey
Grain-size  
Coarse crystalline (2 to 16 mm)
Cohesion  
Strongly cohesive
Water absorption  
Very low
Key constituents  
Biotite
Texture  
Tectonically foliated

Related records


close large map